Journal of Tropical Oceanography ›› 2026, Vol. 45 ›› Issue (2): 42-58.doi: 10.11978/2025104CSTR: 32234.14.2025104
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QIU Cheng1(
), ZHU Yiping2, ZHU Jianrong3(
)
Received:2025-07-14
Revised:2025-07-24
Online:2026-03-10
Published:2026-03-26
Contact:
ZHU Jianrong. email: jrzhu@sklec.ecnu.edu.cn
Supported by:CLC Number:
QIU Cheng, ZHU Yiping, ZHU Jianrong. Changes and causes of saltwater intrusion patterns in the Changjiang Estuary[J].Journal of Tropical Oceanography, 2026, 45(2): 42-58.
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Fig. 2
Shorelines of the Changjiang Estuary in 2007 and 2021. The black dots in the figure represent the measuring stations; the red dots represent the model output points in the North Branch; the red lines divide the North Branch into four areas. S1 and S2 are the transects of the upper and lower reaches of the North Branch; S3 and S4 are the transects of the middle and upper reaches of the North Channel; S5 is the transect in the Hengsha Channel"
Fig. 8
Temporal variations of surface salinity at the water intake of Dongfeng Xisha Reservoir (a), Taicang Reservoir (b), Chenhang Reservoir (c), and Qingcaosha Reservoir (d). The red line represents the year 2021 and the black line represents the year 2007. The green dashed line indicates the salinity threshold"
Tab. 3
Net water flux, net salt flux and water diversion ratio across the North Branch transect S1 during spring tide, middle tide after spring tide, neap tide, middle tide after neap tide and the whole tidal cycles in February 2007 and 2021"
| 统计时段 | 净水通量/(m3·s-1) | 净盐通量/(kg·s-1) | 分流比/% | |||
|---|---|---|---|---|---|---|
| 2021年 | 2007年 | 2021年 | 2007年 | 2021年 | 2007年 | |
| 大潮 | 49 | -374 | -0.01 | -10.07 | 0.41 | -3.07 |
| 大潮后中潮 | 249 | -226 | 0.00 | -5.56 | 1.77 | -1.68 |
| 小潮 | 445 | 76 | 0.00 | -1.10 | 3.03 | 0.55 |
| 小潮后中潮 | -2 | -446 | 0.00 | -9.02 | -0.02 | -4.06 |
| 全潮 | 173 | -224 | 0.00 | -5.94 | 1.36 | -1.81 |
Tab. 4
Tidal prism during spring tide, middle tide after spring tide, neap tide, middle tide after neap tide and the full tidal cycles across the transect S2 in the North Branch and transect S3 in the North Channel in February under the river regime conditions of 2007 and 2021 (unit: ×108m3)"
| 统计时段 | 北支 | 北港 | ||
|---|---|---|---|---|
| 2007 | 2021 | 2007 | 2021 | |
| 大潮 | 9.82 | 6.94 | 16.51 | 14.59 |
| 大潮后中潮 | 8.11 | 5.52 | 13.29 | 11.48 |
| 小潮 | 5.44 | 3.46 | 10.56 | 8.70 |
| 小潮后中潮 | 8.80 | 6.45 | 15.54 | 13.71 |
| 全潮 | 6.63 | 4.43 | 10.28 | 8.93 |
Tab. 5
Net water flux, net salt flux and water diversion ratio across the North Channel transect S4 during spring tide, middle tide after spring tide, neap tide, middle tide after neap tide and the full tidal cycles in February 2007 and 2021"
| 统计时段 | 净水通量/(m3·s-1) | 净盐通量/(kg·s-1) | 分流比/% | |||
|---|---|---|---|---|---|---|
| 2021 | 2007 | 2021 | 2007 | 2021 | 2007 | |
| 大潮 | 8611 | 7754 | 0.18 | 2.46 | 73.53 | 60.74 |
| 大潮后中潮 | 10118 | 8759 | 0.18 | 7.03 | 70.50 | 60.55 |
| 小潮 | 10938 | 9559 | 0.09 | 5.51 | 69.40 | 61.61 |
| 小潮后中潮 | 5708 | 5567 | 0.17 | 1.46 | 63.52 | 55.22 |
| 全潮 | 8693 | 7660 | 0.16 | 4.11 | 68.74 | 58.90 |
Tab. 6
Net water flux and net salt flux across the transect S5 of Hengsha Channel during spring tide, middle tide after spring tide, neap tide, middle tide after neap tide and the full tidal cycles in February 2007 and 2021"
| 统计时段 | 净水通量/(m3·s-1) | 净盐通量/(kg·s-1) | ||
|---|---|---|---|---|
| 2021 | 2007 | 2021 | 2007 | |
| 大潮 | -2041 | -393 | -17.65 | -2.84 |
| 大潮后中潮 | -1859 | -94 | -15.69 | -2.07 |
| 小潮 | -1122 | -412 | -11.19 | -4.24 |
| 小潮后中潮 | -1367 | -230 | -10.62 | -3.62 |
| 全潮 | -1566 | -226 | -13.59 | -2.99 |
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